Titlebook: Basement Tectonics 9; Australia and Other M. J. Rickard,H. J. Harrington,P. R. Williams Conference proceedings 1992 Springer Science+Busin

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Nietzsche and the Battle Over Being,of lithology, deformation, metamorphism and mineralisation..From local applications at ore-deposit scale, the use of lineament tectonics extends to the comparison between lineament-related crustal patterns at continental scale and similar features visible in sea-floor topography and atmospheric patt

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https://doi.org/10.1057/978-1-137-52856-8ine at least five different subduction zones with a growth rate of about 20% of the modern global rate. These subduction zones are also indicated by the shallow crustal lithologies, by poly-metallic mineralization, and by oxygen-isotope and heat-flow data and by geophysical and geochemical behaviour

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Heidegger et le problème de la mortdeposits, Silurian post-orogenic granite plutons, and a syndepositional mid-Proterozoic graben fault. These major features have a persistent N-S orientation (360±100°), suggesting that an extensional E-W stress field has been reactivated many times. Linears can also be identified with E-W, NW-SE, an

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https://doi.org/10.1007/978-3-031-05817-2ose found in the Perth Basin, Western Australia. The orientation of the faults in the Perth Basin can be attributed to reactivation of basement structures during sinistral transtension associated with NE-SE extension. A change to dextral transtension is suggested immediately prior to break-up in the

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